Carbon Burial in Young Tropical Reservoirs Is Higher at Lower Latitudes*  

作　　者：Elizabeth Sikar Marco Aurelio dos Santos Ana Carolina Moterani Isabella Matvienko Ana Carla Martins Veras Juliana Pinto Pereira Dias Orleno Marques da Silva Junior Claudio Pavani Marcelo Amorim Teodosio das Neves Milisse Nzualo Ayr Manoel Portilho Bentes Junior Rogerio Duarte Elizabeth Sikar;Marco Aurelio dos Santos;Ana Carolina Moterani;Isabella Matvienko;Ana Carla Martins Veras;Juliana Pinto Pereira Dias;Orleno Marques da Silva Junior;Claudio Pavani;Marcelo Amorim;Teodosio das Neves Milisse Nzualo;Ayr Manoel Portilho Bentes Junior;Rogerio Duarte(Construmaq São Carlos, São Carlos, SP, Brazil;Programa de Planejamento Energético da Universidade Federal do Rio de Janeiro, Brazil;Laboratório de Energias Renováveis e Estudos Ambientais da Universidade Federal do Rio de Janeiro, Brazil;Instituto de Pesquisas Científicas e Tecnológicas do Estado do Amapá, Brazil;Programa de Pós-Graduação em Geografia da Universidade Federal do Amapá, Brazil)

机构地区：[1]Construmaq Sã o Carlos, Sã o Carlos, SP, Brazil [2]Programa de Planejamento Energético da Universidade Federal do Rio de Janeiro, Brazil [3]Laboratório de Energias Renováveis e Estudos Ambientais da Universidade Federal do Rio de Janeiro, Brazil [4]Instituto de Pesquisas Científicas e Tecnológicas do Estado do Amapá, Brazil [5]Programa de Pós-Graduaç ã o em Geografia da Universidade Federal do Amapá, Brazil

出　　处：《Journal of Geoscience and Environment Protection》2021年第12期84-99,共16页地球科学和环境保护期刊（英文）

摘　　要：Man-made environments such as tropical hydroelectric reservoirs alter the preexisting carbon (C) cycle and remove C from circulation through burial in sediments. Carbon burial (CB) was measured using the silica-tracer method during four field surveys in the less than six-year-old Belo Monte tropical reservoir. Fresh C sedimentation was also measured. Belo Monte’s CB median rate 276 (n = 84;min 0;max 352,625 mg C&#183;m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>1}) is within the range (230 to 436 mg C<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>1}) of CB rates measured further downstream at the Xingu Ria and higher than the averaged over 50 years oceanic rate 244 mg C<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d<sup><span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FMan-made environments such as tropical hydroelectric reservoirs alter the preexisting carbon (C) cycle and remove C from circulation through burial in sediments. Carbon burial (CB) was measured using the silica-tracer method during four field surveys in the less than six-year-old Belo Monte tropical reservoir. Fresh C sedimentation was also measured. Belo Monte’s CB median rate 276 (n = 84;min 0;max 352,625 mg C&#183;m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>1}) is within the range (230 to 436 mg C<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>1}) of CB rates measured further downstream at the Xingu Ria and higher than the averaged over 50 years oceanic rate 244 mg C<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>m^{<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#FFFFFF;">&#45;</span>2}<span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F7F7F7;">&#183;</span>d<sup><span style="color:#4F4F4F;font-family:-apple-system, "font-size:16px;white-space:normal;background-color:#F

关 键 词：Carbon BURIAL SEDIMENTS Hydroelectric Reservoirs 

分 类 号：TP3[自动化与计算机技术—计算机科学与技术]